..., province of Salzburg, Austria. The associated sulfosalts are lillianite–gustavite, heyrovskyite, eskimoite, vikingite, ourayite, bismuthinite, krupkaite, benjaminite, pavonite, and cosalite. Traces of pyrite, tetradymite and native gold also are present. The new species occurs as isolated grains intimately...

... the fluctuations in the average homologue number N across the crystal. This yielded compositional fluctuations of the order of 70-170 Aa over a 1800 Aa region of the crystal, with a 202 Aa lamella of ordered vikingite. Trends in the randomness of the gustavite-vikingite intergrowth were evaluated and the dominant...

..., terrywallaceite, vikingite and treasurite) most frequently as grain aggregates and replacement rims of earlier Ag–Pb–Bi minerals, growing together in aggregates up to 200 × 50 μm. It typically occurs in a close association with Ag,Bi-bearing galena and terrywallaceite. Holubite is opaque, steel-grey in colour...

...Fig. 3. Staročeskéite (Sta), gustavite (Gus) and vikingite (Vik), BSE image of holotype sample ST 37. Galena (white) is the earliest mineral. A fragment for SC-XRD analysis of staročeskéite was extracted from the area marked by white lines. ...

... S 6 ), (ii) phases within solid solution field of heyrovskyite, and (iii) compositions which best correspond to "schirmerite", sensu Makovicky and Karup-Moller (1977b), but may represent disordered gustavite, vikingite or eskimoite. Some of the analysed lillianite homologues contain excess Cu, which...

... of coherence along (010). A lamella, ~24 Å wide, consistent with cosalite or vikingite, within lillianite, is indicated by an empty arrow. ...

...)/2. The lillianite group contains both orthorhombic ( N 1 = N 2) and monoclinic ( N 1 ≠ N 2) members, including lillianite, ( 4,4 L) and vikingite, ( 4,7 L) (see Pring et al ., 1999 for a full list of natural members of the series). Gustavite AgPbBi 3 S 6 is also a 4,4 L homologue and forms...

...F ig . 3. The 8 Å crystal structure of vikingite, an example of a lillianite homologue for which N 1 ≠ N 2 . These are new, unpublished crystallographic data rather close to the original composition and structure determination. ...

...Fig 1. BSE image of sample ST 37 with gustavite Gus 83–86 , vikingite Vik 49 and Vik 59 andAnd 71 49 . The superscript denotes Bi/(Bi + Sb) × 100, the subscript denotes gustavite substitution percentage L%, samples with Bi/(Bi + Sb) ≥ 0.5 are arbitrarily labelled Gus, samples with Bi/(Bi + Sb...

... also non-sulfides and, e.g., the so-called post-perovskite MgSiO 3 phase is actually the 1,1 L member of the family ( Olsen et al. 2008 ). The same family includes also the members with two unequal slabs, like 4,7 L lillianite homologue vikingite ( Makovicky et al. 1992 ). The largest so-far...

... , S. ( 1977 b): Chemistry and crystallography of the lillianite homologous series. II. Definition of new minerals: eskimoite, vikingite, ourayite and treasurite. Redefinition of schirmerite and new data on the lillianite–gustavite solid-solution series . Neues Jahrb. Mineral., Abh . 131 , 56...

... and crystallography of the lillianite homologous series. II. Definition of new minerals: eskimoite, vikingite, ourayite and treasurite. Redefinition of schirmerite and new data on the lillianite–gustavite solid solution series . Neues Jahrb. Mineral., Abh . 131 , 56 – 82 . Makovicky , E. Mumme , W.G...

... Galenobismutite (PbBi 2 S 4 )   Tennantite Ashamalmite (Pb 6 Bi 2 S 9 )     Vikingite (Ag 5 Pb 8 Bi 13 S 30 )     Bismuthine (Bi 2 S 3 )     Wittichenite (Cu 5 BiS 3 )     Hammarite (Cu 2 Pb 2 Bi 4 S 9 )     Benjaminite (AgCu) 3 (BiPb) 7 S 12     Cannizzarite (Pb 8 Bi 10 S 23...